“…Formula (6) allows calculating the solvent flux through the membrane when applying both direct current and a concentration drop. At the same time, for the electroosmotic and osmotic permeability of an ideal negatively charged (cation-exchange) membrane, we have the following formulae, respectively, where F 0 is the Faraday constant, are the diffusion coefficients of cations and anions in the electrolyte solution at infinite dilution, m 0 is the macroscopic porosity of the membrane, is the characteristic exchange capacity of the membrane system [ 32 , 33 , 34 , 35 ], k D is the specific hydrodynamic permeability of the ionite grain (gel), µ o is the viscosity of the solution.…”